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- W2100058981 abstract "The second-order dispersion model developed by A. F. B. Tompson and W. G. Gray (1986a, b) is applied to two porous media problems: one-dimensional solute transport in a packed column and two-dimensional transport in a relatively uniform groundwater aquifer. The importance of the convective source q in the model is recognized, and estimates for its constitutive coefficients β1 and β2 are found through a series of numerical experiments. For the slow-flow problems considered, the diffusive source s seems best represented through a one-term source (K0F) relationship only, instead of a general three-term approximation found earlier. Use of K0 in the column test as predicted from the pipe tests of A. F. B. Tompson and W. G. Gray (1986b) works well if the characteristic length for the Peclet number is chosen to be a typical pore diameter. This procedure did not work well in the aquifer test because of the inconsistency of applying a parameter found in a one-dimensional experiment to a two-dimensional problem. Both the second-order model and the traditional first-order (Fickian) approximation were satisfactory in the tracer tests considered, the former verifying the latter." @default.
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- W2100058981 date "1986-12-01" @default.
- W2100058981 modified "2023-09-22" @default.
- W2100058981 title "A second-order approach for the modeling of dispersive transport in porous media: 3. Application to two porous media problems" @default.
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- W2100058981 doi "https://doi.org/10.1029/wr022i013p01959" @default.
- W2100058981 hasPublicationYear "1986" @default.
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